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188 FIGURE 2.—Locations of late Pliocene fossil localities discussed in the text. SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY HAILE 7C FIGURE 3.—Paratypical humeri of Amplibuteo concordatus from Florida: A, left humerus (UF 165542) from Inglis 1C, Citrus County; B, left humerus (UF 159407) from Haile 7C, Alachua County. For each specimen, scale=xl, bar=l cm.
NUMBER 89 189 carpal trochlea relatively small (carpometacarpus larger, metacarpal I relatively smaller, with distinct proximal curvature, fossa below pisiform shallow and broad, area of internal ligamental fossa relatively greater in Amplibuteo woodwardi («=4) and A. hibbardi). Coracoid with relatively short, narrow coraco-humeral surface (long and broad in A. woodwardi {n=5), short and broad in .4. hibbardi); pneumatic foramina below brachial tuberosity small and indistinct (shallow to deep in A. woodwardi). Humerus (Figure 3) with internal tuberosity relatively narrow and less blunt (large and blunt in A. woodwardi («=9), rounded in A. hibbardi); distinct excavation at distal end of medial bicipital crest (deep in A hibbardi; deep to shallow or absent in A. woodwardi); ligamental furrow relatively narrow and deep (furrow broad, shallow to deep in A. woodwardi); bicipital crest merges with shaft immediately below pneumatic foramen (merges with shaft more distal to pneumatic foramen, forming a distinct flange, in A. woodwardi and A. hibbardi); attachment for anterior articular ligament relatively flat, long, and narrow (flat to convex, short and broad to long and narrow in A. woodwardi, short and rounded in A. hibbardi); impression of M. brachialis anticus relatively narrow (broad in A. woodwardi); and entepicondylar and ectepicondylar prominences relatively small (larger and more robust in A. woodwardi). Ulna with bicipital attachment relatively high on shaft (attachment more distal on shaft in A. woodwardi («=3) and A. hibbardi); prominence for anterior articular ligament relatively small (large and robust in A. woodwardi and A. hibbardi); distal external condyle relatively long and narrow (short and broad in A. woodwardi and A. hibbardi); and carpal and radial tuberosities prominent (reduced in A. woodwardi, more prominent in A. hibbardi). Radius with ligamental prominence relatively small and blunt (large with more distal extension in A. woodwardi («=2) and ,4. hibbardi); scapholunar facet in distal view relatively short and narrow (long and broad in A. woodwardi). COMPARATIVE MATERIAL.—Morphnus guianensis (Daudin), skeleton, USNM 432243, unsexed; LACM 91788, skeleton, female. Harpyhaliaetus solitarius (Tschudi), partial skeleton with sternum, coracoid, proximal humerus, and femur, UCLA 41971, unsexed. STATUS.—Extinct, known from fossils only. REMARKS.—The material from Haile 7C is probably from a single individual based on similarities in the size and features of matching elements. At least one individual is represented from Inglis 1C, and the humerus (UF 165542) is slightly porous and incompletely ossified, indicating it is from a subadult. Amplibuteo concordatus was a small eagle compared to A. woodwardi ox A. hibbardi. A third possible species of Amplibuteo (UF 102550), reported by Emslie (1995) from the late-early Irvingtonian Leisey Shell Pit 3B, is slightly larger than A. concordatus and smaller than A. woodwardi (see measurements in Emslie, 1995, table 11). It compares most closely with A. woodwardi except for the carpometacarpus, which is shorter and differs in characters as described by Emslie (1995). The carpometacarpus (UF 102550) from Leisey was compared with UF 159426 and AMNH 10395 and was found to differ in having a distinct proximal curvature of metacarpal I and having the fossa below the pisiform process broad and deep. These differences also suggest that the Leisey specimen represents a fourth, undescribed species of Amplibuteo. Of the two other fossil species described in this genus, A. woodwardi is known from the late Pleistocene of Rancho La Brea, California, and the middle and late Pleistocene of Florida (Miller, 1911; Howard, 1932; Emslie, 1995); A. hibbardi is known only from the late Pleistocene Talara Tar Seeps, Peru (Campbell, 1979). The addition of A. concordatus to this record extends the geologic range of the genus into the late Pliocene. This species also was relatively long-lived, with a potential geologic range spanning 2.1 million years (between 3.7-1.6 Ma). The genus reached its greatest diversity in the Pleistocene of North and South America, when up to three species may have existed, although none of these apparently were sympatric based on the available evidence. Campbell (1979) erected the genus Amplibuteo, with A. hibbardi of Peru as the type species, and at the same time transferred the fossil species Morphnus woodwardi from Rancho La Brea to the same new genus. His comparisons suggested that Amplibuteo is most closely related to Buteo and Geranoaetus, whereas Morphnus is closer to Harpia than to other genera. Campbell's comparisons included one specimen of Harpyhaliaetus solitarius, from which only the tarsometatarsus was used in the generic diagnosis of Amplibuteo. We compared the sternum, coracoid, proximal end of the humerus, and femur of this species with those of Morphnus guianensis, Amplibuteo woodwardi, and A. concordatus. These comparisons indicate a closer similarity in skeletal characters between Harpyhaliaetus and Amplibuteo than previously has been recognized. Characters shared by these two genera include the sternum with the anterior carinal margin placed relatively far from the manubrium, the coracoid with the coracoidal fenestra positioned relatively far from the scapular facet, the humerus with a bicipital crest that merges with the shaft distally, giving the crest a distinct flange in A. woodwardi (although the crest merges immediately to a shaft with no flange in A. concordatus and Harpyhaliaetus), and the femur with a high trochanter and a trochanteric ridge extending far down the shaft. These similarities raise the possibility that Amplibuteo may be closely related to or even congeneric with Harpyhaliaetus, of which additional modern skeletal specimens would be highly desirable. The high diversity of Accipitridae and the lack of adequate comparative skeletons for some species (e.g., H. coronatus), however, compound the problems associated with describing new taxa in this group, and additional, more detailed comparisons are needed with all accipitrid genera. The two species of Harpyhaliaetus are today confined to the Neotropics. The Crowned Solitary Eagle {H. coronatus) is found in savannah habitats from Bolivia to southern Argentina, whereas the Black Solitary Eagle {H. solitarius) occurs on mountain
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- Page 165 and 166: NUMBER 89 155 the period studied. T
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- Page 184 and 185: 174 ated with this specimen, see Mi
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- Page 221 and 222: NUMBER 89 211 FIGURE 1.—Argornis
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- Page 225 and 226: NUMBER 89 215 caput humeri perpendi
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- Page 229 and 230: NUMBER 89 219 FIGURE 2.—Selmes ab
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- Page 243 and 244: NUMBER 89 233 Subfamily ANATALAVINA
- Page 245 and 246: NUMBER 89 235 mal was found under t
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NUMBER 89 189<br />
carpal trochlea relatively small (carpometacarpus larger,<br />
metacarpal I relatively smaller, with distinct proximal curvature,<br />
fossa below pisiform shallow and broad, area of internal<br />
ligamental fossa relatively greater in Amplibuteo woodwardi<br />
(«=4) and A. hibbardi). Coracoid with relatively short, narrow<br />
coraco-humeral surface (long and broad in A. woodwardi<br />
{n=5), short and broad in .4. hibbardi); pneumatic foramina below<br />
brachial tuberosity small and indistinct (shallow to deep in<br />
A. woodwardi). Humerus (Figure 3) with internal tuberosity<br />
relatively narrow and less blunt (large and blunt in A. woodwardi<br />
(«=9), rounded in A. hibbardi); distinct excavation at<br />
distal end of medial bicipital crest (deep in A hibbardi; deep to<br />
shallow or absent in A. woodwardi); ligamental furrow relatively<br />
narrow and deep (furrow broad, shallow to deep in A.<br />
woodwardi); bicipital crest merges with shaft immediately below<br />
pneumatic foramen (merges with shaft more distal to pneumatic<br />
foramen, forming a distinct flange, in A. woodwardi and<br />
A. hibbardi); attachment for anterior articular ligament relatively<br />
flat, long, and narrow (flat to convex, short and broad to<br />
long and narrow in A. woodwardi, short and rounded in A.<br />
hibbardi); impression of M. brachialis anticus relatively narrow<br />
(broad in A. woodwardi); and entepicondylar and ectepicondylar<br />
prominences relatively small (larger and more robust<br />
in A. woodwardi). Ulna with bicipital attachment relatively<br />
high on shaft (attachment more distal on shaft in A. woodwardi<br />
(«=3) and A. hibbardi); prominence for anterior articular ligament<br />
relatively small (large and robust in A. woodwardi and A.<br />
hibbardi); distal external condyle relatively long and narrow<br />
(short and broad in A. woodwardi and A. hibbardi); and carpal<br />
and radial tuberosities prominent (reduced in A. woodwardi,<br />
more prominent in A. hibbardi). Radius with ligamental prominence<br />
relatively small and blunt (large with more distal extension<br />
in A. woodwardi («=2) and ,4. hibbardi); scapholunar facet<br />
in distal view relatively short and narrow (long and broad in<br />
A. woodwardi).<br />
COMPARATIVE MATERIAL.—Morphnus guianensis (Daudin),<br />
skeleton, USNM 432243, unsexed; LACM 91788, skeleton,<br />
female. Harpyhaliaetus solitarius (Tschudi), partial skeleton<br />
with sternum, coracoid, proximal humerus, and femur,<br />
UCLA 41971, unsexed.<br />
STATUS.—Extinct, known from fossils only.<br />
REMARKS.—The material from Haile 7C is probably from a<br />
single individual based on similarities in the size and features<br />
of matching elements. At least one individual is represented<br />
from Inglis 1C, and the humerus (UF 165542) is slightly porous<br />
and incompletely ossified, indicating it is from a subadult.<br />
Amplibuteo concordatus was a small eagle compared to A.<br />
woodwardi ox A. hibbardi. A third possible species of Amplibuteo<br />
(UF 102550), reported by Emslie (1995) from the late-early<br />
Irvingtonian Leisey Shell Pit 3B, is slightly larger than A.<br />
concordatus and smaller than A. woodwardi (see measurements<br />
in Emslie, 1995, table 11). It compares most closely with<br />
A. woodwardi except for the carpometacarpus, which is shorter<br />
and differs in characters as described by Emslie (1995). The<br />
carpometacarpus (UF 102550) from Leisey was compared with<br />
UF 159426 and AMNH 10395 and was found to differ in having<br />
a distinct proximal curvature of metacarpal I and having the<br />
fossa below the pisiform process broad and deep. These differences<br />
also suggest that the Leisey specimen represents a fourth,<br />
undescribed species of Amplibuteo.<br />
Of the two other fossil species described in this genus, A.<br />
woodwardi is known from the late Pleistocene of Rancho La<br />
Brea, California, and the middle and late Pleistocene of Florida<br />
(Miller, 1911; Howard, 1932; Emslie, 1995); A. hibbardi is<br />
known only from the late Pleistocene Talara Tar Seeps, Peru<br />
(Campbell, 1979). The addition of A. concordatus to this<br />
record extends the geologic range of the genus into the late<br />
Pliocene. This species also was relatively long-lived, with a potential<br />
geologic range spanning 2.1 million years (between<br />
3.7-1.6 Ma). The genus reached its greatest diversity in the<br />
Pleistocene of North and South America, when up to three species<br />
may have existed, although none of these apparently were<br />
sympatric based on the available evidence.<br />
Campbell (1979) erected the genus Amplibuteo, with A. hibbardi<br />
of Peru as the type species, and at the same time transferred<br />
the fossil species Morphnus woodwardi from Rancho La<br />
Brea to the same new genus. His comparisons suggested that<br />
Amplibuteo is most closely related to Buteo and Geranoaetus,<br />
whereas Morphnus is closer to Harpia than to other genera.<br />
Campbell's comparisons included one specimen of Harpyhaliaetus<br />
solitarius, from which only the tarsometatarsus was<br />
used in the generic diagnosis of Amplibuteo. We compared the<br />
sternum, coracoid, proximal end of the humerus, and femur of<br />
this species with those of Morphnus guianensis, Amplibuteo<br />
woodwardi, and A. concordatus. These comparisons indicate a<br />
closer similarity in skeletal characters between Harpyhaliaetus<br />
and Amplibuteo than previously has been recognized. Characters<br />
shared by these two genera include the sternum with the<br />
anterior carinal margin placed relatively far from the manubrium,<br />
the coracoid with the coracoidal fenestra positioned relatively<br />
far from the scapular facet, the humerus with a bicipital<br />
crest that merges with the shaft distally, giving the crest a distinct<br />
flange in A. woodwardi (although the crest merges immediately<br />
to a shaft with no flange in A. concordatus and Harpyhaliaetus),<br />
and the femur with a high trochanter and a<br />
trochanteric ridge extending far down the shaft.<br />
These similarities raise the possibility that Amplibuteo may<br />
be closely related to or even congeneric with Harpyhaliaetus,<br />
of which additional modern skeletal specimens would be highly<br />
desirable. The high diversity of Accipitridae and the lack of<br />
adequate comparative skeletons for some species (e.g., H. coronatus),<br />
however, compound the problems associated with describing<br />
new taxa in this group, and additional, more detailed<br />
comparisons are needed with all accipitrid genera. The two<br />
species of Harpyhaliaetus are today confined to the Neotropics.<br />
The Crowned Solitary Eagle {H. coronatus) is found in<br />
savannah habitats from Bolivia to southern Argentina, whereas<br />
the Black Solitary Eagle {H. solitarius) occurs on mountain